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Gold Science and Technology ›› 2020, Vol. 28 ›› Issue (4): 497-508.doi: 10.11872/j.issn.1005-2518.2020.04.066

• Mineral Exploration and Resource Evaluation • Previous Articles     Next Articles

Primary Halo Characteristics and Geological Significance of the Dongjianian Silver Deposit in Lingbao City,Henan Province

Qichao DUAN1(),Xucheng PANG1(),Rui ZONG2,Di HAN1,Yan ZHANG2,Xin ZHANG1   

  1. 1.Institute of Resources and Environment,Henan Polytechnic University,Jiaozuo 454000, Henan,China
    2.No. 2 Institute of Geological & Mineral Resources Survey of Henan, Zhengzhou 450003, Henan,China
  • Received:2020-03-29 Revised:2020-05-13 Online:2020-08-31 Published:2020-08-27
  • Contact: Xucheng PANG E-mail:dqc_hpu@163.com;jpxc@hpu.edu.cn

Abstract:

Dongjianian silver deposit is the only large deposit found in the south metallogenic belt of Xiao-qinling ore-gathering area. In order to coordinate with the smooth development of the deep exploration of the deposit,the change rule of the useful elements in the vertical direction of the deposit was understood,and the primary halo geochemical method was adopted to determine the change trend of the deep orebody by studying the primary halo characteristics of the typical ore deposit profile. By the analysis of mathematical statistics,and Ag has significant correlation elements Au,Cu,Pb,Zn,As,Sb,W,Ag content of elements is the main source of F1 factor As,Ag,Pb,Au,Zn,Sb element combination,is the main ore-forming elements combination,As,Sb element combination is a typical low temperature elements,they were placed in the same combination as the medium temperature elements of Pb,Zn,Ag and Au,explain Dongjianian silver deposit has many times characteristics,ore-forming process secondary source is F2,F4 factor. Finally,9 elements such as As,Sb,Ag,Au,Cu,Pb,Zn,Co and Mo were determined indicator elements. Among them,As and Sb are indicators of leading edge halo,Ag,Au,Cu,Pb and Zn are indicators of near-ore halo,and Co and Mo are indicators of tail halo. The primary halo axial zoning sequence of the main orebody from top to bottom determined by the zoning index is Co-Mo -Cu-Au-Sb-Zn-Pb-Ag-As,showing the phenomenon of “opposite direction zoning”.Combined with the change characteristics of primary halo geochemical parameters,the study on the denudation degree of orebody and the ideal model,it is predicted that the M1-I main orebody still has a large extension to the depth. The research results can be used as a reference for the research and decision of the deep trend of the same type of mineralized geological body in the region.

Key words: primary halo, geochemistry, geological significance, axial zoning, Dongjianian silver deposit, Xiaoqinling

CLC Number: 

  • P618.52

Fig.1

Regional geological map of Dongjianian silver deposit (modified after references[8,21])"

Fig.2

Profile map of No.08 prospecting line"

Table 1

Logarithmic correlation matrix of elements"

元素AgAuCuPbZnAsSbCoWMo
Au0.501.00
Cu0.370.421.00
Pb0.690.410.401.00
Zn0.570.350.510.791.00
As0.600.710.470.580.441.00
Sb0.360.300.260.390.290.541.00
Co-0.020.130.580.090.380.060.011.00
W0.220.090.310.430.470.250.380.291.00
Mo0.050.140.280.000.010.120.030.210.051.00
Bi-0.09-0.29-0.15-0.07-0.16-0.230.08-0.150.14-0.15

Fig.3

R-type cluster analysis pedigree chart of elements"

Table 2

Rotational component factor matrix"

元素成分因子
F1F2F3F4
As0.8790.076-0.0180.208
Ag0.8110.126-0.1710.153
Pb0.7550.3640.126-0.311
Au0.7510.0720.0120.265
Zn0.6600.4660.020-0.314
Sb0.602-0.0050.5310.207
Co-0.1130.862-0.1010.226
Cu0.3860.690-0.0360.321
Bi-0.224-0.1380.781-0.098
W0.2390.5430.671-0.062
Mo0.0430.184-0.0450.801
特征值3.522.161.321.18
方差贡献率/%32.019.712.010.8
累计方差贡献率/%32.051.763.774.5

Table 3

Calculation results of primary halo axial zoning sequence of M1-Ⅰ orebody by Gregorian’s zonality index method"

项目中段AgAuCuPbZnAsSbCoMo
线金属量(W97000000005.850.57
92021.690.7411.96224.24168.240.082.768.154.67
79013.13237.33169.86974.201 704.7034.295.832.473.45
62024.6452.5118.142 427.272 041.2526.412.6100
标准化系数1010010010-110-110102102102
标准化数据9700000000585.4456.93
920216.900.7411.9622.4216.820.80276.00815.44466.93
790131.27237.33169.8697.42170.47342.89582.82247.44344.93
620246.3752.5118.14242.73204.13264.07260.9400
分带指数(D9700.00010.00010.00010.00010.00010.00010.00010.91140.0886
9200.11870.00040.00650.01230.00920.00040.15100.44610.2554
7900.05650.10210.07310.04190.07330.14750.25070.10650.1484
6200.19110.04070.01410.18830.15840.20490.20250.00010.0001
判定系数9701 523
920-1 374
790-1 271-737-2 508
620-3 826-3 771-3 170-4 099
分带序列Co - Mo - Cu - Au - Sb - Zn - Pb - Ag - As

Table 4

Calculation results of primary halo axial zoning sequence of M1-Ⅰ orebody by concentration index method"

项目中段AgAuCuPbZnAsSbCoMo
元素含量9700.510.6629.3112.25124.730.692.2718.413.88
92022.161.4239.28239.93232.560.744.6716.998.79
79013.67233.24197.07976.361 765.8534.877.7011.307.52
62024.0947.5143.062 189.211 820.4732.725.087.743.83
Cˉ15.1170.7177.18854.44985.9017.264.9313.616.00

浓集指数

标准化值

9700.03400.00940.37970.01430.12650.04020.46051.35290.6457
9201.46680.02010.50900.28080.23590.04290.94731.24831.4640
7900.90463.29862.55341.14271.79112.02081.56220.83041.2527
6201.59460.67200.55792.56221.84651.89611.03010.56840.6376
浓集指数(Z9700.09980.02761.11570.04210.37170.11811.35293.97501.8971
9202.12400.02910.73700.40660.34160.06211.37181.80772.1201
7900.53021.93321.49650.66971.04971.18430.91550.48670.7342
6201.26280.53210.44182.02891.46221.50150.81570.45010.5049
判定系数97019.20
920-15.592.175.97
790-132.980.02
620-56.17-9.61-38.17
分带序列Co - Mo- Sb - Ag - Cu - Au - Zn - As - Pb

Table 5

Statistical of the results of the two zonal sequence calculation methods"

矿体分带序列计算方法
M1-ⅠCoMoCuAuSbZnPbAgAs分带指数法
CoMoSbAgCuAuZnAsPb浓集指数法

Fig.4

Change characteristic diagram of element content in each middle section of M1-Ⅰ orebody"

Fig.5

Denudation coefficient and primary halo geochemical ideal model of main orebody M1-Ⅰ in Dongjianian silver deposit"

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